珠江口盆地深水区白云凹陷始新世洼陷结构研究
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摘要
利用新采集的长电缆地震资料及地质、测井和地化资料研究表明,白云凹陷在始新世文昌期由一系列断层控制的半地堑组成,断裂对文昌组沉积的控制作用明显,但晚期白云凹陷的持续沉降以及巨厚的渐新统—中新统地层沉积,掩盖了早期半地堑的形态。断陷期的半地堑控制了湖相烃源岩的分布,对这些半地堑的进一步分析有利于厘清文昌组烃源岩的分布及促进该区的油气勘探。
The structure of Baiyun Sag in the deep-water area of Pearl River Mouth Basin was studied by applying the new long-cable seismic data in combination with the geology, logging and geochemistry data. Baiyun Sag was composed of a series of half-grabens controlled by the faults in the Wenchang Age of Eocene Epoch, and the sediment of Wenchang Formation was controlled by faults obviously in this period. In the Late Eocene Epoch, Baiyun Sag persisted subsiding and deposited the thick strata of the Oligocene-Miocene, which covered the early structure of half-grabens. In the rift period, the half-grabens controlled the distribution of lacustrine source rocks. Further analysis to half-grabens is favorable to reveal the distribution of source rocks in Wenchang Formation and improve the petroleum exploration in this area.
引文
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